Lecture 11 Evapotranspiration (4) - PowerPoint PPT Presentation

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Lecture 11 Evapotranspiration (4)

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Lecture 11 Evapotranspiration (4) ET Measurements Lysimeters Evaporation Pans Pan size effects Lysimeter Weighing Lysimeters Draining Lysimeters Evaporation Pan (US ... – PowerPoint PPT presentation

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Title: Lecture 11 Evapotranspiration (4)


1
Lecture 11 Evapotranspiration (4)
ET Measurements
  • Lysimeters
  • Evaporation Pans
  • Pan size effects

2
Lysimeter
  • Allow determination of water balance of a block
    of soil
  • Maintain wet soil to measure PET
  • Allow soil moisture to fluctuate to measure AET
  •  

http//lawr.ucdavis.edu/classes/
hyd143/hyd143week2.html
3
Weighing Lysimeters
  • Use a balance to assess changes in storage
  • Small lysimeters can be removed and weighed
  • Measure both PET and AET

http//www.kfa-juelich.de/icg/icg5/irapic/einlasse
.jpg
4
Draining Lysimeters
  • Soil block is isolated but must be undisturbed
    and in the same surroundings
  •  
  • Cant measure change in storage, only inputs and
    outputs

http//www.l-sadwrn.dircon.co.uk/ lysim.html
5
Evaporation Pan (US Class A)standard of the
National Weather Service (NWS)
http//www.fao.org/docrep/S2022E/s2022e07.htm
6
Sunken Colorado Pan
http//www.fao.org/docrep/S2022E/s2022e07.htm
7
Evaporation Pans
Solve a simplified water-balance equation for a
given period (?t)
E W (V2 V1)
E Evaporation W Precipitation during ?t V1
Volume at beginning of ?t V2 Volume at end of
?t  
8
Estimating the Effect of Pan Size
Empirical equations to account for energy
exchange through the side the pan, in order to
estimate free water evaporation
when Tspan gt Ta - when Tspan lt Ta  
Efw Evaporation from free-water surface Epan
Pan evaporation P Atmospheric pressure
(mb) vpan Avg. wind speed 15 cm above pan
(km/day) Tspan Water-surface temperature
(?C) Ta Air temperature (?C) ?pan Proportion
of energy lost to evaporation
Kohler et al. (1955)
9
Evaporation Pans
  • Free-water evaporation
  • Expose a cylindrical (or rectangular) pan of
    water to the atmosphere
  • Provide estimates of potential
    evapotranspiration (PET) can be more accurate
    than formulae
  • Must be related to vegetation canopies using
    other methods (coefficients etc.)
  • Precipitation is measured in an adjacent rain
    gauge
  • Pan volume is measured by recording water height
    (which is maintained by adding or removing
    measured amounts of water)
  • Pans can be placed on land in clearings or on
    floating platforms on open water and usually
    surrounded by fences

10
Plot Studies
  • Water balance approach applied to small
    undisturbed plots of land
  • Analogous to small lake for simple evaporation
  • Must select suitable sites where inputs/outputs
    can be measured
  • Spatial uncertainty increases with size of plot
  • Artificial rain (sprinklers) can be used to
    assess PET
  • Soil moisture assessed by spot sampling and
    measurement by
  • Gravimetric methods
  • Soil block moisture
  • Neutron probe
  • Time domain reflectometry

11
Catchment Studies
  • Water balance of entire drainage basin
  • Even greater spatial uncertainties
  •   Variable precipitation, soil water capacity
  • Ground water seepage
  •  
  • Better for long term estimates
  • On a yearly basis, change in storage is
    approx. zero
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